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Water Quality Monitoring for the Sustainable Management of
Aquatic Ecosystem in the Markandeya Dam Reservoir, Kolar
District, Karnataka, India
Gayathri S., Tejushree H. S., Yashaswini R., Shashikumar C., Shravani. K
Water Quality Research Unit, Department of Zoology, Bangalore University JB Campus, Bengaluru
560056, Karnataka, India
DOI: https://doi.org/10.51583/IJLTEMAS.2026.150600224
Received: 12 July 2026; Accepted: 17 July 2026; Published: 25 July 2026
ABSTRACT
Water is an irreplaceable natural resource and the cornerstone of aquatic and terrestrial ecosystems alike. Dams
and reservoirs are critical infrastructure that support biodiversity, agriculture, potable water supply, hydropower
generation, flood mitigation, and recreation. Despite their ecological importance, reservoir water quality remains
vulnerable to seasonal fluctuations, anthropogenic pollution, and nutrient enrichment. The present study
evaluates the physico-chemical characteristics and plankton community structure of Markandeya Dam, Kolar
District, Karnataka, India, across pre-monsoon, monsoon, and post-monsoon seasons from February to July
2025. Phytoplankton (22 taxa) and zooplankton (14 taxa) were enumerated and subjected to nine diversity
indices. A Water Quality Index (WQI) computed via the Weighted Arithmetic Index method yielded a value of
46.57, classifying the reservoir as moderately polluted. Nygaard's Water Quality Indices (NWQI) further
indicated a mesotrophic trophic status. Most physico-chemical parameters conformed to WHO and BIS
drinking-water standards; however, dissolved oxygen variability and elevated faecal coliform counts signal
localized organic pollution and microbial contamination risks. ShannonWiener diversity indices for both
phytoplankton (H' = 01.45) and zooplankton (H' = 00.92) indicated moderate pollution, with dominance by
Chlorophyceae and Monogononta rotifers, respectively. Seasonal patterns revealed higher diversity and species
richness during cooler pre-monsoon months and greater dominance during warm transitional periods. The
integration of WQI, NWQI, and multi-index plankton assessment constitutes a robust and replicable framework
for the ecological monitoring and sustainable management of tropical reservoir ecosystems.
Keywords: Physico-chemical parameters; Water Quality Index; Nygaard's Water Quality Indices;
Phytoplankton diversity; Zooplankton community; Mesotrophic reservoir; Kolar District; Karnataka
INTRODUCTION
Water is fundamental to life, shaping public health, economic productivity, and the structural integrity of natural
ecosystems. Although approximately 71% of the Earth's surface is covered by water, only a minute fraction exists as
accessible freshwater, rendering inland water bodies of exceptional ecological and socio-economic significance (Miller &
Lake, 2014). Reservoirs and dam systems are engineered freshwater ecosystems that simultaneously serve as water-supply
infrastructure and as habitats for diverse aquatic communities. They regulate streamflow, recharge groundwater, support
irrigation, enable hydropower, and provide recreational and cultural services (Johnson & Wang, 2020).
Despite these multifaceted services, reservoirs are susceptible to a range of stressors that progressively degrade water
quality and ecological function. Anthropogenic pressuresincluding agricultural runoff carrying nutrients and pesticides,
untreated sewage discharge, land-use change in catchment areas, and increasing human water demandexacerbate natural
seasonal fluctuations in temperature, precipitation, and nutrient dynamics (Chen et al., 2021; Smith et al., 2018). The
cumulative outcome is nutrient loading, eutrophication, dissolved-oxygen depletion, and microbial contamination, all of
which compromise the use of reservoir water for drinking, fisheries, and agriculture.
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Plankton communities are sensitive ecological indicators of water quality and trophic status. Phytoplanktoncomprising
diatoms, green algae, cyanobacteria, and dinoflagellatesoccupy the base of the aquatic food web and mediate oxygen
production and carbon cycling (Falkowski & Raven, 2007).
Zooplankton link primary producers to higher trophic levels and modulate phytoplankton biomass through grazing
pressure (Balseiro et al., 2023; Mohammed et al., 2023). The composition and diversity of both groups respond rapidly to
environmental perturbations, making them ideal biomonitors (Kour et al., 2022; Enawgaw et al., 2023).
The Water Quality Index (WQI) is a widely adopted aggregation tool that distils multiparametric physico-chemical data
into a single dimensionless score, facilitating public communication and decision-making (Horton, 1965).
Nygaard's Water Quality Indices (NWQI) complement WQI by providing a phytoplankton-based assessment of trophic
state (Hutchinson, 1967, after Nygaard, 1949). Together, these frameworks deliver a comprehensive picture of reservoir
health that neither chemical nor biological approaches achieve in isolation.
Regional studies have documented varied water quality conditions in South Indian reservoirs. Manjare et al. (2010)
characterised the physico-chemistry of Tamdalge tank in Maharashtra, while Basavaraj and Kadadevaru (2024) evaluated
physico-chemical parameters and zooplankton in Gopalaswamy tank, Chitradurga. Asulabha et al. (2022) catalogued
phytoplankton diversity across Bangalore lakes, identifying 58 genera.
Farnaz and Rahmatullah (2021) and Garg (2022) have similarly characterised water quality in Bihar and Haryana ponds,
respectively, using physico-chemical indices. However, Markandeya Dama historically significant irrigation and water-
supply reservoir in Kolar District, Karnatakaremains poorly characterised with respect to integrated biological and
chemical monitoring.
The present study therefore aims to: (i) characterise seasonal variation in physico-chemical water quality across pre-
monsoon, monsoon, and post-monsoon periods; (ii) assess phytoplankton and zooplankton community structure and
diversity; (iii) determine the Water Quality Index and Nygaard trophic classification; and (iv) identify monitoring and
management priorities for sustainable utilisation of the reservoir's water resources.
Description of the Study Area
Markandeya Dam is situated at geographic coordinates 16°2'0" N, 74°38'30" E, near Budikote village in Malur Taluk,
Kolar District, Karnataka, India (Fig. 1).
Constructed between 1936 and 1940, the dam impounds the Markandeya River, which bifurcates in the vicinity of the
structure. The crest elevation is 30 m, the dam wall extends 750 m in length, and the surrounding terrain lies at an average
elevation of approximately 794 m above mean sea level.
The reservoir has a storage capacity of 553.61 TMC ft and drains a catchment area of approximately 19.71 km². It was
constructed at a project cost of Rs. 43.20 crore with the primary objective of supplying potable and irrigation water to 184
villages in Bangarpet Taluk via a 14 km pipeline extending to Tekal village.
The region experiences a semi-arid tropical climate characterised by a hot dry season (MarchMay), a southwest monsoon
(JuneSeptember), and a mild post-monsoon winter (OctoberFebruary), with mean annual rainfall of approximately 750
mm.
The dam's catchment is predominantly agricultural, with crops of ragi, groundnut, and vegetables. Human settlements,
livestock grazing, and the absence of a buffer zone around the reservoir margin render the water body vulnerable to non-
point-source pollution. The study was conducted at a single representative sampling station located near the dam wall at
a depth of 0.51.0 m, representing the principal water abstraction zone.
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Figure : 1 Location map of Markandeya Dam.
MATERIALS AND METHODS
Sample Collection and Preservation Physico-chemical Analysis
Water samples were collected monthly from February to July 2025, covering post-monsoon (February), early pre-monsoon
(MarchMay), onset of monsoon (June), and mid-monsoon (July) periods. Surface grab samples were collected at 0.5 m
depth between 08:00 and 09:00 h using acid-washed 1 L polyethylene containers. All containers were pre-rinsed three
times with sample water prior to collection. Samples were labelled with site, date, and time to prevent misidentification.
Temperature and pH were measured in situ using a calibrated mercury glass thermometer and a portable digital pH meter
(±0.01 unit resolution), respectively. Remaining samples were transported on ice to the laboratory and analysed within 24
h following the Standard Methods for the Examination of Water and Wastewater (APHA, 2005).
Parameters determined in the laboratory included total dissolved solids (TDS; gravimetric method), electrical conductivity
(EC; conductivity bridge), dissolved oxygen (DO; Winkler's iodometric titration), biochemical oxygen demand (BOD; 5-
day BOD test at 20°C), chemical oxygen demand (COD; dichromate reflux method), chloride (argentometric titration),
total alkalinity (titrimetric method), total hardness (EDTA complexometric titration), phosphate (molybdenum blue
spectrophotometric method), nitrate (UV spectrophotometry at 220 nm), sulphate (barium sulphate turbidimetric method),
and faecal coliform (membrane filtration technique). All reagents were of analytical grade.
Sample Collection and Preservation Plankton Analysis
Plankton samples were collected concurrently with physico-chemical samples. Qualitative and quantitative phytoplankton
samples were collected using a 25 µm mesh plankton net via both vertical and horizontal hauls. For quantitative
enumeration, unconcentrated phytoplankton samples were collected from beneath the surface at 0.5 m depth, while
zooplankton samples were obtained at 1.0 m depth. All plankton samples were preserved immediately in Lugol's iodine
solution (1% final concentration). Plankton cells and organisms were counted under a compound microscope using a
Sedgwick-Rafter (S-R) counting cell. Identification to genus and species level was conducted following APHA (2005)
standard taxonomic keys.
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Statistical and Index Analyses
Physico-chemical data were analysed using SPSS v. 16.0 (SPSS Inc., Chicago, IL, USA). Pearson's correlation coefficients
(r) were computed to evaluate pairwise relationships among the 15 parameters. The Water Quality Index (WQI) was
determined following the Weighted Arithmetic Index (WAI) method of Horton (1965), comprising four steps: (i)
parameter selection, (ii) sub-index (Q-value) generation, (iii) weight factor (Wi) assignment, and (iv) aggregation to a
composite WQI score. The trophic status of the reservoir was determined using Nygaard's Composite Quotient and
associated algal indices (Hutchinson, 1967, after Nygaard, 1949).
Plankton diversity was characterised using nine indices computed in PAST v. 4.0 (Hammer et al., 2001): ShannonWiener
diversity index (H'), Simpson's diversity index (1 D), Pielou's evenness (J'), Dominance index (D), Menhinick's richness
index, Margalef's richness index, Fisher's alpha index, and the BergerParker dominance index. Water quality
interpretation of H' values followed the classification of Wilhm and Dorris (1968): H'> 3 = clean water; 1 H' 3 =
moderate pollution; H'< 1 = heavy pollution.
RESULTS
Physico-chemical Parameters
Monthly variation in the 15 physico-chemical parameters measured from February to July 2025 is presented in Table 1.
Atmospheric temperature ranged from 28.0°C to 29.0°C (mean 28.73 ± 0.40°C), reflecting the consistently warm tropical
climate of the study region. Water temperature tracked atmospheric temperature closely, ranging from 26.0°C to 30.5°C
(mean 27.83 ± 1.91°C); peak values in AprilMay are consistent with pre-monsoon solar heating, while monsoon season
values (JuneJuly) were moderated by cloud cover and rainfall. These temperature ranges are within the tolerance limits
of most tropical freshwater organisms.
Water pH fluctuated between 6.0 (May) and 8.0 (June) with a mean of 7.00 ± 0.70, spanning near-neutral to slightly
alkaline conditions. All values fell within the BIS permissible range (6.58.5) for drinking water, indicating adequate
buffering capacity. TDS ranged from 248 to 289 mg/L (mean 272.50 ± 16.40 mg/L), substantially below the BIS
acceptable limit of 500 mg/L, affirming low mineralisation and good palatability. Electrical conductivity (EC) ranged
from 370.14 to 431.34 µS/cm (mean 406.71 ± 24.49 µS/cm), commensurate with the TDS values and consistent with
freshwater systems of low ionic strength.
Dissolved oxygen (DO) exhibited the greatest variability of any parameter, ranging from 1.0 mg/L (July) to 10.4 mg/L
(May), with a mean of 4.06 ± 3.34 mg/L. Values below 4 mg/L, observed in February and July, represent hypoxic
conditions that can compromise aerobic aquatic life; the peak in May likely reflects intense algal photosynthesis during a
bloom event. BOD ranged from 1.0 to 4.4 mg/L (mean 2.46 ± 1.16 mg/L), indicating moderate biodegradable organic
loading. COD showed wider fluctuation (1.625.6 mg/L; mean 11.73 ± 8.56 mg/L), with the February peak (25.6 mg/L)
suggesting elevated non-biodegradable organic or chemical inputs during the post-monsoon residual period.
Chloride concentrations were low (4860 mg/L; mean 55.16 ± 4.66 mg/L), well within the BIS limit of 250 mg/L, ruling
out significant saline or sewage influence on ion balance. Total alkalinity exhibited the highest coefficient of variation of
all parameters (range: 8348 mg/L; mean 123.66 ± 122.66 mg/L), with the June peak (348 mg/L) likely reflecting
concentration of bicarbonates from catchment weathering following the onset of monsoon inflow. Total hardness ranged
from 28 to 204 mg/L (mean 76.33 ± 67.85 mg/L), indicative of soft to moderately hard water. Phosphate concentrations
remained low (0.01.0 mg/L; mean 0.41 ± 0.37 mg/L), as did nitrate (010 mg/L; mean 2.50 ± 4.18 mg/L)both well
below WHO thresholds. Sulphate ranged from 8 to 26 mg/L (mean 19.00 ± 7.01 mg/L), far below the BIS acceptable limit
of 200 mg/L.
Faecal coliform counts ranged from 126 to 450 cfu/100 mL (mean 297.33 ± 106.48 cfu/100 mL). These levels substantially
exceed the WHO guideline of 0 cfu/100 mL for drinking water and 100 cfu/100 mL for recreational use, indicating
significant faecal contamination attributable to open defecation, livestock watering, and surface runoff from agricultural
fields in the catchment.
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Table : 1 - Monthly variation in physico-chemical parameters of Markandeya Dam, Kolar District, Karnataka (February
July 2025).
Sl.
No.
Parameter
Feb
Mar
Apr
May
Jun
Jul
Max
Min
1
Atm. Temperature (°C)
28.5
29.0
29.0
29.0
28.9
28.0
29.0
28.0
28.73 ± 0.40
2
Water Temperature (°C)
26.0
26.5
30.0
30.5
27.0
27.0
30.5
26.0
27.83 ± 1.91
3
pH
7.5
6.5
7.0
6.0
8.0
7.0
8.0
6.0
7.00 ± 0.70
4
TDS (mg/L)
286
278
289
277
248
257
289
248
272.50 ± 16.40
5
EC (µS/cm)
426.9
414.9
431.3
413.4
370.1
383.6
431.3
370.1
406.71 ± 24.49
6
DO (mg/L)
1.8
4.0
4.2
10.4
3.0
1.0
10.4
1.0
4.06 ± 3.34
7
BOD (mg/L)
2.6
2.4
1.0
4.4
2.8
1.6
4.4
1.0
2.46 ± 1.16
8
COD (mg/L)
25.6
9.6
9.6
1.6
6.4
17.6
25.6
1.6
11.73 ± 8.56
9
Chloride (mg/L)
60
60
55
56
52
48
60
48
55.16 ± 4.66
10
Total Alkalinity (mg/L)
106
80
8
36
348
164
348
8
123.66 ±
122.66
11
Total Hardness (mg/L)
42
102
28
46
204
36
204
28
76.33 ± 67.85
12
Phosphate (mg/L)
0.5
0.5
0.5
0.0
1.0
0.0
1.0
0.0
0.41 ± 0.37
13
Nitrate (mg/L)
0.0
10.0
0.0
5.0
0.0
0.0
10.0
0.0
2.50 ± 4.18
14
Sulphate (mg/L)
20
26
26
8
14
20
26
8
19.00 ± 7.01
15
Faecal Coliform
(cfu/100 mL)
450
320
260
342
126
286
450
126
297.33 ±
106.48
Biostatistical (Correlation) Analysis
Pearson's correlation matrix revealed several ecologically meaningful parameter relationships. A significant positive
correlation between water temperature and DO (r = 0.631) suggests that photosynthetic oxygen production by
phytoplankton, rather than physical dissolution, governs DO during warmer months. The positive pHCOD correlation (r
= 0.423) implies that organic matter decomposition under alkaline conditions drives chemical oxygen demand. The
positive CODsulphate association (r = 0.426) may reflect anaerobic sulphate reduction mediated by organic substrates
during stratification.
Strong negative correlations were observed for pH–nitrate (r = −0.676) and pH–DO (r = −0.720), indicating that elevated
biological activity and carbon dioxide production during algal blooms can suppresses pH while concurrently depleting
dissolved oxygen. The positive DOnitrate correlation (r = 0.444) is consistent with nitrification processes that occur
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under aerobic conditions. The total hardnessphosphate correlation (r = 0.588) likely reflects geochemical co-leaching of
calcium, magnesium, and phosphorus from catchment soils during high-intensity monsoon rainfall events.
Water Quality Index (WQI)
The WQI was computed for seven key parameters using the Weighted Arithmetic Index method; results are summarised
in Table 2. The water quality index (WQI) was calculated using weighted arithmetic index (WAI) approach (refer equation
1,2 and 3). The objective of water quality index was originally proposed by Horton (1965). A commonly-used water
quality index (WQI) was developed by the National Sanitation Foundation (NSF) in 1970 (Brown et al. 1970). Parameters
as dissolved oxygen, fecal coliforms, pH, biological oxygen demand, phosphate, nitrate and total dissolved solids were
recognized as preliminary indication of quality as is used in calculating quality index. In the present study the composite
WQI score of 46.57 classifies the reservoir as 'moderately polluted' water.
Table : 2 - Water Quality Index (WQI) determination for Markandeya Dam, Kolar District, Karnataka (Weighted
Arithmetic Index method; Horton, 1965).
Sl.
No.
Parameter
Unit
Estimated
Value (Mi)
Q-Value
(Qi)
Weight
Factor (Wi)
WiQi
WQI
1
DO
mg/L
4.006
124.175
0.166
20.613
46.57
(Moderate)
2
Faecal Coliform
cfu/100
mL
297.33
235.900
0.0079
1.864
3
pH
7.000
0.000
0.105
0.000
4
BOD
mg/L
2.46
41.000
0.166
6.806
5
Phosphate
mg/L
0.41
8.200
0.200
1.640
6
Nitrate
mg/L
2.50
5.550
0.022
0.122
7
TDS
mg/L
272.5
54.500
0.002
0.109
∑Wi = 0.668 ∑WiQi = 31.154
Q
i
= M
i
I
i
X 100 (1)
S
i
- I
i
Where : Q
i
= quality rating corresponding to the i
th
parameter is a number reflecting the relative value of the
parameter, M
i
= estimated values of the parameters in the laboratory, I
i
= Ideal values of the i
th
parameter (ideal
values are taken as zero except for pH = 7 and DO =14) and S
i
= standard values of the i
th
parameter.
W
i
= k (2)
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S
i
Where : W
i
= unit weight ; k = 1 ; S
i
= recommended standards of the corresponding parameter .
WQI = ∑W
i
Q
i
(3)
∑W
i
Where : WQI = the overall water quality index.
Table : 3 - Correlation of physico-chemical parameters in Markandeya Dam during Feb-July 2025
*Correlation is significant at the 0.05 level (2-tailed)
**Correlation is significant at the 0.01 level (2-tailed)
AT
WT
pH
TDS
EC
DO
BO
D
CO
D
Chlorid
e
TA
TH
Phospha
te
Nitrate
Sulpha
te
FC
AT
1
.469
-.242
.334
.334
.631
.323
-.701
.532
-.215
.323
.412
.468
-.070
-.220
WT
1
-.554
.312
.312
.777
.203
-.667
-.108
-.523
-.354
-.370
.000
-.328
-.117
pH
1
-.431
-.431
-.720
-.365
.423
-.242
.749
.534
.751
-.676
.121
-.401
TDS
1
1.000
*
*
.268
-.092
.191
.736
-.885
*
-.675
-.219
.226
.391
.703
EC
1
.268
-.092
.192
.736
-.885
*
-.675
-.219
.226
.391
.704
DO
1
.723
-.755
.248
-.435
-.119
-.345
.444
-.591
.083
BOD
1
-.428
.270
.057
.211
-.167
.370
-.843
*
.182
COD
1
.117
.004
-.357
-.033
-.402
.426
.558
Chloride
1
-.472
-.110
.180
.538
.226
.610
TA
1
.835
*
.588
-.341
-.291
-.646
TH
1
.777
.074
-.226
-.709
Phosphat
e
1
-.159
.189
-.511
Nitrate
1
.102
.202
Sulphate
1
.108
FC
1
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Table : 4 - The rating of the Trophic state Indices of Nygaard’s is presented below:
4.4 Phytoplankton Community and Diversity
A total of 22 phytoplankton taxa were identified from Markandeya Dam across the study eperiod. The taxonomic
composition was dominated by Chlorophyceae (10 taxa), followed by Cyanophyceae (3 taxa), Bacillariophyceae (2 taxa),
Zygnematophyceae (1 taxon ), Oligohymenophora (1 taxon), Tubulinea (1 taxon), Ulvophyceae (2 taxa), Dinophyceae (1
taxon), and Chrysophyceae (1 taxon). The percentage composition of the phytoplankton groups are shown in Figure : 2.
Phytoplankton diversity indices revealed pronounced seasonality. The ShannonWiener index (H') peaked at 1.45 in
February (moderate pollution) and fell to 0 in June (heavy pollution), indicating low diversity. The Dominance index
reached 1 in May, corresponding to a near-monoculture bloom, while the BergerParker index confirmed that a single
taxon constituted 50100% of the community depending on season. Margalef's richness was highest in February (1.35)
and collapsed to 0 in May, consistent with bloom-induced competitive exclusion of minor taxa. Fisher's alpha was highest
in Feb (1.8). Collectively, the indices indicate pre-monsoon as the period of highest ecological resilience and monsoon-
onset as a period of ecological stress or bloom disturbance.
Asulabha et al. (2022) reported 58 phytoplankton genera across Bangalore lakes, indicating substantially higher regional
phytoplankton richness than observed in Markandeya Dam (22 taxa). The comparatively lower richness in the present
study may reflect the semi-arid location of Kolar District and the relatively shallow, fluctuating nature of the reservoir.
Table : 5 - Diversity index of Phytoplankton Group in Markandeya dam during Feb July 2025
Feb
March
April
May
June
July
Taxa_S
7
6
5
1
3
3
Individuals
85
105
117
68
102
132
Dominance_D
0.3188
0.3968
0.3927
1
0.5002
0.5005
Shannon_H
1.456
1.152
1.125
0
0.7563
0.7773
Simpson_1-D
0.6812
0.6032
0.6073
0
0.4998
0.4995
Evenness_e^H/S
0.6124
0.5275
0.6159
1
0.7101
0.7252
Menhinick
0.7593
0.5855
0.4623
0.1213
0.297
0.2611
Margalef
1.351
1.074
0.84
0
0.4324
0.4096
Equitability_J
0.748
0.6431
0.6988
0.6884
0.7075
Fisher_alpha
1.808
1.381
1.061
0.1662
0.5796
0.5463
Berger-Parker
0.5059
0.5238
0.5128
1
0.5882
0.6061
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Zooplankton Community and Diversity
Fourteen zooplankton taxa were identified, with a community heavily dominated by Monogononta rotifers (7 taxa;
77% of total taxa), including Brachionus calyciflorus and Keratella cochlearis as codominant species. Additional
groups comprised Eurotatoria (3 taxa; 14%), Maxillopoda copepods (3 taxa; 5%), and Crustacea (1 taxon; 8%). The
predominance of hardy, pollution-tolerant rotifers is characteristic of eutrophic or anthropogenically stressed
freshwater systems in which rapid rotifer reproduction confers a competitive advantage over more sensitive
crustacean zooplankton (Kour et al., 2022; Enawgaw et al., 2023).
Zooplankton ShannonWiener diversity was consistently low (H' = 0.250.92), peaking in April (H' = 0.92) and
falling to its lowest in May (H' = 0.25). Dominance was complete in February and March (Dominance index = 1.0;
BergerParker index = 1.0), consistent with single-species rotifer dominance during cooler, drier conditions. The
Margalef index increased from 0 in FebruaryMarch to 0.70 in July, suggesting monsoon-driven recruitment of taxa
from inflowing streams. These patterns parallel those of phytoplankton and reinforce the narrative of seasonal
community restructuring driven by temperature, hydrology, and trophic dynamics.
Numerous investigations have demonstrated the utility of zooplankton as ecological and water quality indicators in
tropical reservoirs (Imoobe & Akoma, 2008; Beyene et al., 2022; Ginatullina et al., 2023; Oh et al., 2023; Ndah et
al., 2022; Rashid & Prakash, 2022). The present findings corroborate this body of evidence: low zooplankton
diversity, rotifer dominance, and depressed crustacean presence collectively signal moderate ecological stress and
water quality degradation in Markandeya Dam.
Feb
March
April
May
June
July
Taxa_S
1
1
3
2
3
4
Individuals
2
10
34
28
69
70
Dominance_D
1
1
0.455
0.8673
0.5026
0.5751
Shannon_H
0
0
0.9291
0.2573
0.8596
0.8449
Simpson_1-D
0
0
0.545
0.1327
0.4974
0.4249
Evenness_e^H/S
1
1
0.8441
0.6467
0.7874
0.5819
51%
25%
12%
7%
0%
0%
3%
0%
2%
Figure : 2 - Percentage composition of Phytoplankton in
Markandeya Dam during Feb-July 2025
Chlorophyceae
Cyanophyceae
Bacillariophyceae
Zygnematophyceae
Oligohymenophorea
Tubulinea
Ulvophyceae
Dinophyceae
Chrysophyceae
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Menhinick
0.7071
0.3162
0.5145
0.378
0.3612
0.4781
Margalef
0
0
0.5672
0.3001
0.4724
0.7061
Equitability_J
0
0
0.8457
0.3712
0.7825
0.6095
Fisher_alpha
0.7959
0.2766
0.7935
0.493
0.6396
0.9208
Berger-Parker
1
1
0.6176
0.9286
0.6667
0.7429
Table : 6 - Diversity indices of Zooplankton group in Markandeya Dam during Feb-July 2025
DISCUSSION
The physico-chemical profile of Markandeya Dam broadly conforms to acceptable standards for freshwater reservoirs
in tropical India, with most parameters within BIS and WHO limits. The reservoir can be characterised as a low-
mineralisation, near-neutral to slightly alkaline system with moderate organic loadinga profile consistent with its
semi-arid, largely agricultural catchment. However, several parameters warrant management attention.
Dissolved oxygen variability (1.010.4 mg/L) is the most ecologically critical finding from the physico-chemical
survey. Hypoxic conditions (<4 mg/L) in February and July likely reflect decomposition of accumulated organic
matter during post-monsoon stagnation and monsoon-onset stratification, respectively. Such conditions can trigger
fish kills, promote anaerobic decomposition pathways, and release sediment-bound phosphorus, potentially triggering
internal nutrient loading and accelerating eutrophicationa feedback loop widely documented in shallow tropical
reservoirs (Johnson & Wang, 2020).
Faecal coliform counts exceeding 126450 cfu/100 mL represent the most acute water quality concern for human
health. These values indicate persistent faecal contamination exceeding WHO recreational and drinking-water
guidelines by 12 orders of magnitude. The contamination pathway is most plausibly diffuse: open defecation and
livestock access to the reservoir margin, combined with surface runoff from periurban agricultural areas. Without
source-control interventions, the dam water requires multi-barrier treatment (coagulation, filtration, and chlorination)
prior to domestic use.
Figure : 3 - Percentage composition of Zooplankton
In Markandeya Dam during Feb-July s2025
5%
7%
Monogononta
Euratatoria
14%
Crustacea
Maxillopoda
74%
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The WQI value of 46.57 is situated in the 'moderately polluted' band (2650), confirming that the reservoir is not
pristine but retains ecological and utilitarian value. Nygaard's trophic indices, corroborated by Chlorophyceae
dominance and cyanobacterial co-occurrence in phytoplankton, consistently classify the reservoir as mesotrophic.
Mesotrophy represents a transitional trophic state that, under continued nutrient loading, may shift toward eutrophy
a trajectory observed in many peri-urban South Indian reservoirs (Asulabha et al., 2022). The integrated WQINWQI
framework provides a more complete assessment than either approach in isolation, as WQI captures chemical hazards
and NWQI reflects biological nutrient status.Bloom-forming cyanobacteria produce cyanotoxins that are hazardous
to livestock, fish, and humans and are resistant to conventional water treatment (Falkowski & Raven, 2007).
Zooplankton rotifer dominance and suppression of cladocerans and copepodsthe primary phytoplankton grazers
signal a trophic cascade that may reduce top-down control of algal biomass. In less-disturbed oligotrophic to
mesotrophic systems, cladocerans such as Daphnia provide substantial phytoplankton grazing pressure; their absence
or scarcity in Markandeya Dam may allow phytoplankton biomass to accumulate unchecked during nutrient-rich
monsoon periods. Restoring zooplankton community structure through reduction of anthropogenic nutrient loading
could therefore yield co-benefits for algal control.
The seasonal pattern of increasing diversity in February (pre-monsoon winter) and declining diversity in MayJune
(hot season and monsoon onset) is consistent with the intermediate disturbance hypothesis, under which intermediate
levels of physical disturbance (thermal mixing in winter) promote coexistence, while thermal stratification and bloom
events suppress it. This pattern has ecological management implications: pre-monsoon monitoring windows capture
maximum biodiversity and therefore offer the most sensitive baseline for detecting chronic pollution impacts.
CONCLUSION
This study provides the first comprehensive integrated assessment of water quality and plankton biodiversity in
Markandeya Dam, Kolar District, Karnataka. The principal conclusions are as follows:
(1) Most physico-chemical parameters conform to BIS and WHO standards, supporting the reservoir's potential for
irrigation and treated drinking water supply; however, dissolved oxygen variability and elevated faecal coliform
counts (297.33 ± 106.48 cfu/100 mL) indicate persistent organic pollution and microbial contamination that require
immediate remediation.
(2) A composite WQI of 46.57 classifies Markandeya Dam as moderately polluted water. Nygaard's trophic
assessment categorises the reservoir as mesotrophic, with a risk of eutrophication progression under continued
anthropogenic pressure.
(3) Twenty-two phytoplankton and 14 zooplankton taxa were recorded. Shannon diversity indices (H' = 01.45 and
H' = 00.92, respectively) and taxonomic composition confirm moderate pollution conditions, with Chlorophyceae
and Monogononta rotifers as diagnostic dominants.
(4) Seasonal diversity maxima in February and minima in MayJune reflect the interplay of temperature, thermal
stratification, and bloom dynamics, with pre-monsoon periods providing the most sensitive monitoring window.
(5) The concurrent application of WQI, NWQI, and multi-index plankton biodiversity assessment constitutes a
replicable, cost-effective framework for the ecological surveillance and sustainable management of tropical dam
reservoirs.
Management recommendations include: installation of riparian buffer strips to intercept agricultural runoff;
prohibition of livestock access to the reservoir margin; construction of community sanitation facilities in surrounding
villages; regular cyanotoxin monitoring during pre-monsoon bloom periods; and long-term quarterly monitoring to
detect trophic trajectory shifts. Future investigations should extend the sampling period to a full hydrological year,
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incorporate sediment nutrient analysis, and employ molecular (metabarcoding) approaches to enhance taxonomic
resolution of the plankton community.
Declarations
Funding
This research received no specific grant from funding agencies in the public, commercial, or not-for-profit sectors.
Conflicts of Interest
The authors declare no conflicts of interest.
Author Contributions
Gayathri S.: Conceptualisation, Methodology, Formal Analysis, Writing Original Draft. Tejushree H. S.: Sample
Collection, Laboratory Analysis. Yashaswini R.: Data Curation, Validation. Shashikumar C.: Supervision, Shravani.
K. Writing Review and Editing.
Data Availability Statement
The datasets generated and analysed during the current study are available from the corresponding author upon
reasonable request.
Ethical Approval
This study involved water and plankton sample collection from a public reservoir and did not involve vertebrate
animals requiring ethical committee approval. Field sampling was conducted in compliance with local environmental
regulations.
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